Am. Gabelnick et al., Molecular mechanisms of propyne oxidation on the Pt(111) surface: In situ soft X-ray studies in pressures of oxygen, J PHYS CH B, 105(32), 2001, pp. 7748-7754
Oxidation of preadsorbed propyne has been characterized on the Pt(111) surf
ace in oxygen at pressures up to 0.009 Torr using fluorescence yield ultras
oft X-ray adsorption methods above the carbon K edge. A combination of temp
erature-programmed reaction spectroscopy (TPRS) and temperature-programmed
fluorescence yield near edge spectroscopy (TP-FYNES) experiments indicating
that similar oxidation pathways occur both for coadsorbed oxygen and press
ures of oxygen. Soft X-ray spectroscopy indicates that propyne's pi system
adsorbs nearly parallel to this surface with a saturation coverage of 1.45
x 10(15) C atoms/cm(2). Oxidation of small propyne coverages with coadsorbe
d oxygen results in simultaneous CO2 and H2O peaks at 320 and 420 K, as see
n in TPRS. Oxidation of higher propyne coverages with coadsorbed oxygen res
ults in a broad oxidation peak over the 350-420 K temperature range. Oxidat
ion of a saturated propyne monolayer in oxygen pressures (TP-FYNES) results
in a rapid decrease in carbon coverage over the same temperature range, su
ggesting similar mechanisms. Isothermal oxidation in oxygen atmospheres ind
icates that propyne oxidation is first-order in propyne coverage and has an
activation energy of 17 kcal/mol for high coverages. Deviations from first
-order behavior suggest that a second process may become important at lower
coverages in oxygen atmospheres. Regardless of coverage and initial condit
ions, both TPRS and TP-FYNES indicate oxydehydrogenation and skeletal oxida
tion occur simultaneously and the oxidation proceeds with a fixed C3H4 stoi
chiometry. Taken together, these results give a molecular picture of propyn
e oxidation on the Pt(111) surface.